Tracking millennial-scale Holocene glacial advance and retreat using osmium isotopes: Insights from the Greenland ice sheet

Rooney, A.D.; Selby, D.; Lloyd, J.M.; Roberts, D.H.; Lückge, A.; Sageman, B.B.; Prouty, N.G.

doi:10.1016/j.quascirev.2016.02.021

Tracking millennial-scale Holocene glacial advance and retreat using osmium isotopes: Insights from the Greenland ice sheet

Rooney, A.D.; Selby, D.; Lloyd, J.M.; Roberts, D.H.; Lückge, A.; Sageman, B.B.; Prouty, N.G.

Authors

A.D. Rooney

Professor David Selby
Professor

Professor Jeremy Lloyd j.m.lloyd@durham.ac.uk
Professor

Professor Dave Roberts d.h.roberts@durham.ac.uk
Professor

A. Lückge

B.B. Sageman

N.G. Prouty

Abstract

High-resolution Os isotope stratigraphy can aid in reconstructing Pleistocene ice sheet fluctuation and elucidating the role of local and regional weathering fluxes on the marine Os residence time. This paper presents new Os isotope data from ocean cores adjacent to the West Greenland ice sheet that have excellent chronological controls. Cores MSM-520 and DA00-06 represent distal to proximal sites adjacent to two West Greenland ice streams. Core MSM-520 has a steadily decreasing Os signal over the last 10 kyr (187Os/188Os = 1.35–0.81). In contrast, Os isotopes from core DA00-06 (proximal to the calving front of Jakobshavn Isbræ) highlight four stages of ice stream retreat and advance over the past 10 kyr (187Os/188Os = 2.31; 1.68; 2.09; 1.47). Our high-resolution chemostratigraphic records provide vital benchmarks for ice-sheet modelers as we attempt to better constrain the future response of major ice sheets to climate change. Variations in Os isotope composition from sediment and macro-algae (seaweed) sourced from regional and global settings serve to emphasize the overwhelming effect weathering sources have on seawater Os isotope composition. Further, these findings demonstrate that the residence time of Os is shorter than previous estimates of ∼104 yr.

Citation

Rooney, A., Selby, D., Lloyd, J., Roberts, D., Lückge, A., Sageman, B., & Prouty, N. (2016). Tracking millennial-scale Holocene glacial advance and retreat using osmium isotopes: Insights from the Greenland ice sheet. Quaternary Science Reviews, 138, 49-61. https://doi.org/10.1016/j.quascirev.2016.02.021

Journal Article Type	Article
Acceptance Date	Feb 19, 2016
Online Publication Date	Mar 8, 2016
Publication Date	Apr 15, 2016
Deposit Date	Feb 19, 2016
Publicly Available Date	Mar 8, 2017
Journal	Quaternary Science Reviews
Print ISSN	0277-3791
Publisher	Elsevier
Peer Reviewed	Peer Reviewed
Volume	138
Pages	49-61
DOI	https://doi.org/10.1016/j.quascirev.2016.02.021

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Publisher Licence URL
http://creativecommons.org/licenses/by-nc-nd/4.0/

Copyright Statement
© 2016 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license
(http://creativecommons.org/licenses/by/4.0/)